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Half-Life Calculator

Use the half-life equation N = N₀ × (1/2)t/t½ to find the amount left after a given time, the starting amount, the time elapsed or the half-life itself, with the decay constant, mean lifetime and half-lives of common isotopes.
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What do you want to find?
Solve for
Amounts

Any quantity proportional to the number of nuclei works: mass, activity or count rate

Time

Results

Remaining amount (N)
25g
N = 100 × (1/2)^(2)
Fraction remaining
75 g decayed
25%
Half-lives elapsed
Over 10 y
2
Half-life used
5 y
Decay constant (λ = ln 2 ÷ t½)
0.1386per year
Mean lifetime (τ = t½ ÷ ln 2)
7.213y

Remaining amount (N): 25 g

Decay schedule
Half-livesTimeRemainingPercent
00 y100 g100%
15 y50 g50%
210 y25 g25%
315 y12.5 g12.5%
420 y6.25 g6.25%
525 y3.125 g3.125%
630 y1.563 g1.563%
735 y0.7813 g0.781%
840 y0.3906 g0.391%
945 y0.1953 g0.195%
1050 y0.09766 g0.098%

Decay is random for each nucleus; this formula gives the expected amount for a large number of atoms. Times use a year of 365.25 days.

How to use the half-life calculator

  1. Choose the unknown: remaining amount, initial amount, time, or half-life.
  2. Pick an isotope to fill in its half-life, or enter your own half-life and unit. Any exponentially decaying quantity works, including drug levels or a cooling-off model.
  3. Enter the amounts in any unit (grams, percent, becquerels, counts per minute). Both amounts use the same unit, so only their ratio matters.
  4. Enter the time and its unit. The results include the decay constant, the mean lifetime and a schedule for ten half-lives.

Half-life formulas

N(t) = N₀ × (1/2)t ÷ t½ = N₀ × e−λt
λ = ln 2 ÷ t½  ·  τ = 1 ÷ λ = t½ ÷ ln 2
t = t½ × log₂(N₀ ÷ N)
t½ = t × ln 2 ÷ ln(N₀ ÷ N)

N₀ is the starting amount, N the amount left after time t, and t½ the half-life: the time for half of the remaining nuclei to decay. The decay constant λ is the probability per unit time that a given nucleus decays, and the mean lifetime τ is the average time a nucleus survives, about 1.443 half-lives. Because every half-life removes half of what is left, after 10 half-lives only 0.098% remains.

Worked examples

  • Iodine-131: with a half-life of 8.0252 days, 100 g left for 30 days decays to 100 × (1/2)30 ÷ 8.0252 = 7.49 g.
  • Radiocarbon dating: a sample with 25% of its original carbon-14 is two half-lives old: 2 × 5,700 = 11,400 years. After 1,000 years, 88.55% of the carbon-14 remains.
  • Finding a half-life: if a sample's count rate falls from 1,000 to 250 counts per minute in 16 days, t½ = 16 × ln 2 ÷ ln 4 = 8 days, close to iodine-131.

Half-lives of common isotopes

Half-lives are evaluated nuclear data (ENSDF) from the IAEA Nuclear Data Section's LiveChart of Nuclides, the same evaluations distributed by the US National Nuclear Data Center. The last two columns are computed with the calculator's engine.

IsotopeSymbolHalf-lifeDecayKnown forLeft after 1 yearTime to fall to 1%
Fluorine-18¹⁸F109.77 minutesβ⁺ / electron capturePET scans< 0.000001%12.2 h
Technetium-99m⁹⁹ᵐTc6.0072 hoursIsomeric transitionMedical imaging< 0.000001%1.66 days
Radon-222²²²Rn3.8222 daysαIndoor radon gas< 0.000001%25.4 days
Iodine-131¹³¹I8.0252 daysβ⁻Thyroid treatment; fission product< 0.000001%53.3 days
Phosphorus-32³²P14.266 daysβ⁻Biology labeling1.96 × 10⁻⁶%94.8 days
Iodine-125¹²⁵I59.407 daysElectron captureBrachytherapy, lab assays1.41%1.08 years
Polonium-210²¹⁰Po138.376 daysαStatic eliminators16%2.52 years
Cobalt-60⁶⁰Co1925.28 days (5.27 years)β⁻Radiotherapy, sterilization87.7%35 years
Tritium (hydrogen-3)³H12.32 yearsβ⁻Exit signs, watch dials94.5%81.9 years
Strontium-90⁹⁰Sr28.91 yearsβ⁻Fission product97.6%192 years
Cesium-137¹³⁷Cs30.08 yearsβ⁻Fission product, gauges97.7%200 years
Americium-241²⁴¹Am432.6 yearsαSmoke detectors99.84%2,870 years
Radium-226²²⁶Ra1,600 yearsαHistoric luminous paint99.957%10,600 years
Carbon-14¹⁴C5,700 yearsβ⁻Radiocarbon dating99.988%37,900 years
Plutonium-239²³⁹Pu24,110 yearsαNuclear fuel and weapons99.997%160,000 years
Uranium-235²³⁵U704 million yearsαNuclear fuel> 99.999%4.68 × 10⁹ years
Potassium-40⁴⁰K1.248 billion yearsβ⁻ / electron captureNatural radioactivity, K–Ar dating> 99.999%8.29 × 10⁹ years
Uranium-238²³⁸U4.468 billion yearsαUranium–lead dating> 99.999%2.97 × 10¹⁰ years
Thorium-232²³²Th14.0 billion yearsαNatural radioactivity> 99.999%9.3 × 10¹⁰ years

Where half-lives matter

Medicine favors short half-lives: technetium-99m loses 94% of its activity in a day, long enough for a scan but short enough to limit the patient's dose. Dating needs half-lives on the scale of the ages being measured: after 50,000 years less than 0.3% of the original carbon-14 is left, which is why radiocarbon dating stops working around that age and geologists turn to uranium or potassium isotopes. Waste management follows the same arithmetic: a store of cesium-137 needs about 300 years to fall to 0.1% of its original activity.

Things to know

  • Decay is statistical. No one can say when a single nucleus will decay; the formula describes the average behavior of very many nuclei, which is extremely precise for a gram of material.
  • Activity follows the same curve. Activity in becquerels or curies is proportional to the number of nuclei, so it halves every half-life too.
  • Decay chains. Some products are themselves radioactive (radium-226 decays to radon-222, for example), so total radioactivity can behave differently from one isotope's curve.
  • Seven half-lives leave under 1% (0.78%), a common rule of thumb for when a short-lived medical isotope has effectively gone.
  • This calculator is for learning and planning. Radiation protection decisions should follow your radiation safety officer and official guidance.

The log calculator helps with the logarithms in the time and half-life formulas, and the exponent calculator with powers of ½.

Frequently asked questions

How do you calculate the amount left after a number of half-lives?

Use N = N₀ × (1/2)^(t/t½). 100 g of iodine-131 (half-life 8.0252 days) left for 30 days is 3.74 half-lives, so about 7.49 g remains.

How do I calculate a half-life from measurements?

Use t½ = t × ln 2 ÷ ln(N₀ ÷ N). If a count rate falls from 1,000 to 250 counts per minute in 16 days, that is two halvings, so t½ = 16 × 0.6931 ÷ 1.3863 = 8 days.

How old is a sample with 25% of its carbon-14 left?

Two half-lives. With the evaluated carbon-14 half-life of 5,700 years, that is 11,400 years. Real radiocarbon ages also need calibration for past changes in atmospheric carbon-14.

What is the decay constant?

The decay constant λ = ln 2 ÷ t½ is the fraction of nuclei that decay per unit time. For cesium-137 (half-life 30.08 years) it is about 0.02304 per year. The mean lifetime is its inverse, 1 ÷ λ, or about 1.443 half-lives.

How many half-lives until a substance is gone?

It never reaches exactly zero, but 7 half-lives leave under 1% (0.78%) and 10 half-lives leave about 0.098%. For cesium-137, falling to 1% takes about 200 years.

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